Fault zones in limestones: impact on karstogenesis and groundwater flow (Lez aquifer, southern France)

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Fault zones in limestones: impact on karstogenesis and groundwater flow (Lez aquifer, southern France) V. Clauzon 1 & S. Mayolle 2 & V. Leonardi 1 & P. Brunet 1 & R. Soliva 2 & P. Marchand 1 & G. Massonnat 3 & J.-P. Rolando 3 & S. Pistre 1 Received: 20 July 2019 / Accepted: 21 May 2020 # Springer-Verlag GmbH Germany, part of Springer Nature 2020

Abstract The Lez aquifer in southern France comprises low-porosity karstified limestones and provides drinking water for ~400,000 inhabitants. Population growth and climate change have increased the stress on the water resources. In order to provide long-term protection and to optimize the water supply, the hydrogeology of the Lez aquifer must be better characterized. This study focused particularly on the St-Clément major fault zone (12 km long with a 500-m normal throw) which was structurally characterized using accurate geological mapping of the area, outcrops analysis and geophysics tools. The research highlights and explains the close relationship between the fault and the karstic occurrences. Moreover, tracer tests and piezometric head variations in boreholes have shown (1) strong interconnection between the observed karstic formations and (2) the major role of StClément fault on mass and pressure transfers in the aquifer. At the reservoir scale, the other major faults of the Lez aquifer, such as Corconne-Matelles or Gourg Noir faults, have shown some common morphologic and dynamic characteristics, and suggest a similar hydrogeological functioning. This study then extends this model to a larger scale. It proposes that, in aquifers of lowporosity carbonates, fault zones control the development of the main karstic network which, in turn, controls the main groundwater flows. Thus, faults should be reconsidered in order to improve the vulnerability studies and the quality of karstic aquifer modelling. Therefore, this report can contribute to protecting the groundwater resource, improving yields and optimizing groundwater supply exploitation in this type of aquifer. Keywords Fault zones . Karst . Groundwater flow . France

Introduction The Mediterranean coastal areas support a large and growing population: 95 million inhabitants in 1979; 172 million inhabitants estimated for 2025 (PNUE/PAM 2012). The water resources across the region are subjected to a strong and

Electronic supplementary material The online version of this article (https://doi.org/10.1007/s10040-020-02189-9) contains supplementary material, which is available to authorized users. * V. Clauzon [email protected] 1

HydroSciences Montpellier, UMR 5569, Université de Montpellier, CNRS, IRD, Montpellier, France

2

Geosciences Montpellier, UMR 5243, Université de Montpellier, Université des Antilles, CNRS, Montpellier, France

3

Total S.A., CSTJF, Avenue Larribau, 64018 Pau Cedex, France

increasing demand in a context where climate change causes periods of drought that are becoming longer (e.g. García-Ruiz et al. 2011; Milano et al. 2013; Nunes et al. 2017). The karstic aquifers, which